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Landscapes Forest and Global Change - ESA - Escola Superior ...

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M.L.Leite & J.S.V. Filho 2010. Identification of climatic trends for some localities in the Southern Region of Campos Gerais<br />

384<br />

cities of Lapa <strong>and</strong> Fern<strong>and</strong>es Pinheiro, the latter being significant at 0.01%, while for the city of<br />

Ponta Grossa, the maximum temperature had a significant negative trend of 0.01%. For<br />

minimum temperature, all the cities had significant positive trends, showing a rise in the<br />

minimum temperature in the region. These results of a temperature rise in the southern region of<br />

Campos Gerais, in the State of Parana, is reinforced by analyzing the average temperature in the<br />

three localities, which showed positive trends. Finally, for the city of Ponta Grossa, in despite of<br />

having observed an average temperature rise, this was not significant for the studied period.<br />

4. Discussion<br />

According to Silva (2004) the rainfall in southern Brazil are distributed regularly throughout the<br />

year, compared to other regions of the country, but in recent years the phenomenon El Nino has<br />

served continuously in this region. This climatic phenomenon, when actuates, significantly<br />

alters the levels of rainfall, which are increased during the year. Whereas this phenomenon has<br />

been acting steadily in the region, the increase in the totals of annual rainfall <strong>and</strong> the positive<br />

trend observed for the city of Ponta Grossa may be correlated with the performance of such a<br />

frequent phenomenon in the region. Back (2001) also found elevated totals of annual rainfall for<br />

the city of Urussanga, State of Santa Catarina, identifying a significant positive trend. The<br />

decrease of the maximum temperature in Ponta Grossa, along with higher minimum temperature,<br />

can be partially explained as a consequence of increased cloudiness in the region. Due to this<br />

rise in the levels of cloudiness during the day, a smaller amount of sunlight can reach the earth's<br />

surface, occurring a decrease in maximum temperature. During the night, with lots of clouds,<br />

there is greater retention of radiation, complicating its loss to space, thereby increasing the<br />

minimum temperature at location (Silva & Guetter, 2003). In a previous study, Silveira & Gam<br />

(2006), analyzing changes in minimum temperatures in southern Brazil, found that the<br />

minimum temperature in the state of Rio Gr<strong>and</strong>e do Sul also showed a positive trend over the<br />

study period under review. The same increases were verified by Obregon & Marengo (2007),<br />

which developed a major study on climate throughout the Brazilian territory, in order to<br />

determine possible changes in climate variables. In this study the annual minimum temperatures<br />

in the city of Curitiba, Brazil, showed a significant positive trend at 0.05%, reinforcing the<br />

findings of elevated temperatures in the State of Parana. One reason for this increase in<br />

temperatures can also be correlated to the increase in the totals of areas destinated to<br />

urbanization in the last years (Sansigolo et al., 1992). In some regions, deforestation <strong>and</strong><br />

changes in l<strong>and</strong> use, as a result of human activities have increased rapidly in recent decades, <strong>and</strong><br />

there are evidences that these actions can modify the thermodynamic characteristics of the<br />

lower atmosphere. These changes are the result of complex interactions between climate,<br />

hydrology, vegetation <strong>and</strong> management of water resources <strong>and</strong> l<strong>and</strong>.<br />

Acknowlegments<br />

The authors thank to the Instituto Agronômico do Paraná (IAPAR) for the authorization to<br />

access the rainfall data, <strong>and</strong> to the SETI – Fundação Araucaria, by the research support.<br />

References<br />

Back, J.A., 2001. Aplicação de análise estatística para a identificação de tendências climáticas.<br />

Pesq. Agropec. Bras., 36, n. 5: 717-726.<br />

Groisman, P., Knight, R., Easterling, D., Karl, T., Hegerl, G., Razuvaev, V., 2005. Trends in<br />

tense precipitation in the climate record. Journal of Climate, 18: 1326-1350.<br />

<strong>Forest</strong> <strong>L<strong>and</strong>scapes</strong> <strong>and</strong> <strong>Global</strong> <strong>Change</strong>-New Frontiers in Management, Conservation <strong>and</strong> Restoration. Proceedings of the IUFRO L<strong>and</strong>scape Ecology<br />

Working Group International Conference, September 21-27, 2010, Bragança, Portugal. J.C. Azevedo, M. Feliciano, J. Castro & M.A. Pinto (eds.)<br />

2010, Instituto Politécnico de Bragança, Bragança, Portugal.

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